Table of Contents Author Guidelines Submit a Manuscript
Advances in High Energy Physics
Volume 2013, Article ID 464926, 22 pages
http://dx.doi.org/10.1155/2013/464926
Review Article

Neutrino Oscillations in the Atmospheric Parameter Region: From the Early Experiments to the Present

1Dipartimento di Fisica e Astronomia, University of Bologna, Viale Berti Pichat 6/2, 40127 Bologna, Italy
2INFN, Sezione di Bologna, Viale Berti Pichat 6/2, 40127 Bologna, Italy

Received 15 July 2013; Revised 9 October 2013; Accepted 5 November 2013

Academic Editor: Elisa Bernardini

Copyright © 2013 G. Giacomelli et al. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.

Abstract

The aim of this paper is to provide a historical perspective on the main experimental steps which led to the current picture of neutrino oscillations in the “atmospheric parameter region.” In the 1980s a deficit of atmospheric muon neutrinos was observed with the first generation of underground experiments. In the following decade new experiments provided fundamental results which led to the discovery claims in 1998. At the beginning of the new century neutrino beams of medium and high energy became available and several long baseline experiments were performed and added new information to the atmospheric neutrino puzzle. The interpretation of the results of atmospheric and long baseline neutrino experiments was in terms of dominant oscillations. Short recollections are made of the SNO solar neutrino measurements, of the results with neutrino telescopes, and of reactor neutrinos to measure sin2. Over the years the phenomenological picture improved in completeness and increased in complexity. A short perspective concludes the paper.

1. Introduction

A first hypothesis on neutrino oscillations of the type was introduced in the 50s by Pontecorvo in analogy with strangeness oscillations in the quark sector [1, 2]. Later the idea was extended to include mixing between mass and flavor eigenstates and transitions between different neutrino flavors [3, 4]. Pontecorvo predicted possible variations of the solar flux on Earth due to neutrino oscillations [4].

Experimentally the first indication of a neutrino flux deficit with respect to expectations came from solar neutrinos. Since the late 1960s it was observed that the neutrino flux from the sun measured with a chlorine target experiment [58] was significantly smaller than that computed with theoretical predictions based on the solar standard model (SSM) [9, 10]. The anomaly was confirmed in the 80s by experiments using gallium (GALLEX [11], SAGE [12, 13], and GNO [14]) and water targets (Kamiokande [15, 16]). The deficit—referred to as the “solar neutrino problem”—was interpreted in different ways, in particular, invoking neutrino oscillations, namely, the conversion in flight of solar in other neutrino flavors. The final proof of the solar neutrino problem came in 2001 and 2002 with the results of the SNO heavy-water experiment [17, 18]. Measuring the rates of charged current (CC) interactions (sensitive only to ) and of neutral current (NC) interactions (sensitive to all neutrino flavors) it was proved that the deficit existed only for while the total neutrino flux rate was consistent with the SSM predictions. These results lead to the following conclusions: (i) neutrinos oscillate during their travel toward the Earth, (ii) solar neutrino fluxes are in agreement with the SSM predictions if neutrino oscillations are taken into account, and (iii) it was indirectly proved that neutrino flavors at the detection level are different from those produced at the source. In 2002 the KamLAND experiment [19]—free from the systematics related to solar models—provided a positive indication/evidence for neutrino oscillations in the solar energy sector using artificial beams from a large number of nuclear reactors. More recently, the Borexino experiment at the Gran Sasso Laboratory confirmed the solar oscillation scenario measuring the flux of the low energy Be neutrinos [20, 21].

At another energy scale and much shorter distances, a flux reduction with respect to expectations was observed in the study of atmospheric neutrinos. Incoming high energy primary cosmic rays, protons, or nuclei, interacting with nitrogen and oxygen nuclei in the upper atmosphere, produce pions and kaons, which decay yielding muons and muon neutrinos, in their turn muons decay yielding electrons and muon/electron neutrinos. High energy neutrinos are produced in a spherical layer at 15 km above ground and they proceed towards the Earth. From simple arguments it follows that the ratio of the numbers of muon to electron neutrinos is 2 in a limited energy range and .

The early water Cherenkov detectors IMB [22, 23] and Kamiokande [2426] reported anomalies in the ratio of muon to electron neutrinos, while the tracking calorimeters NUSEX [27], Fréjus [28, 29], and the final Baksan scintillator detector results [30, 31] determined values in agreement with no oscillations. The / ratio anomaly was confirmed by the Soudan-2 experiment [32].

At the Neutrino 1998 Conference in Japan the Soudan-2 [33], MACRO [3437], and Super-Kamiokande (SK) [38] collaborations reported deficits in the muon fluxes from () interactions with respect to Monte Carlo (MC) predictions and distortions in the muon angular distributions; Soudan-2 and Super-Kamiokande also found that the () distributions agreed with MC predictions. These features were explained in terms of oscillations, possibly as , while the channel was excluded as a dominant one.

The atmospheric neutrino flux was computed in the early 1990s [39, 40] and 2000s [4143]. At low energies,  GeV, the predicted number of neutrinos differed by 20–30%. At higher energies, ≥ 10 GeV, the computations were more reliable and had an estimated systematic uncertainty of about 15%. The predicted relative rates of and and the shapes of the zenith distributions were affected by lower systematic errors.

Atmospheric neutrino experiments were mainly disappearance experiments, that is, experiments which measured a reduction of the flux compared with the flux or a depletion in the number of with the distance from production to detection. The observation of the appearance of some ’s in a beam would prove the present paradigm of neutrino oscillations.

This paper is organized as follows. In Section 2 the formalism underlying the phenomenon of neutrino oscillations is recalled. Section 3 is devoted to the atmospheric neutrino experiments, separated on a historical basis into “early” experiments, experiments in the “discovery” phase, and precise confirmation accelerator experiments. In Section 4 are discussed the measurements with reactor antineutrinos of the mixing angle and in Section 5 are described the results from the long baseline neutrino oscillation experiments operating in the “atmospheric parameter region” (K2K, NuMi, and CNGS). Section 5.1 is dedicated to the LSND scale and to a discussion of new proposals on the subject of sterile neutrinos. In Section 6 we review existing experimental results which cannot be accommodated in the standard neutrino oscillation framework. In Section 7 are briefly summarized the present experimental efforts to measure neutrino cross sections and kinematical quantities useful for a correct interpretation of the neutrino data. In Section 8 are examined the roles that large neutrino telescopes could have in the framework of neutrino oscillations. We conclude in Section 9 with comments on some important open issues in neutrino physics.

2. Neutrino Oscillations and Masses

The standard model (SM) of particle physics has been experimentally verified to a high degree of accuracy over a broad range of energies and processes [4449]. The SM cosmology has received confirmations from the Planck experiment [50]. The Higgs particle was recently discovered at the CERN LHC by the ATLAS and CMS experiments, using mainly the cleanest decays and charged leptons [51, 52]. The two experiments are now making precise measurements of all the properties to check if the discovered particle is really the Higgs boson of the SM. In the SM, neutrinos are described as massless left-handed (LH) fields (the opposite for antineutrinos which are right-handed, RH). Each LH neutrino is a component of an SU doublet together with the corresponding charged lepton fields. In case of neutrino mixing and nonzero neutrino masses RH neutrinos (and correspondingly LH antineutrinos) form an SU electroweak singlet with no coupling to SM vector bosons (sterile neutrinos).

The existence of neutrino oscillations—and therefore of massive neutrinos—is the first direct and unambiguous evidence for physics beyond the SM. Moreover any theory able to accommodate neutrino masses should provide an explanation for the fermion mass pattern as presently known in the SM, where neutrinos masses are orders of magnitudes smaller than other massive particles (Figure 1). We recall that all particle masses arise from the interactions with the Higgs field. The SM in its present form is not able to predict the mass spectrum illustrated in Figure 1.

464926.fig.001
Figure 1: Masses of leptons, of quarks, and of the Higgs boson and neutrino mass splittings in the solar and atmospheric sectors. The dots for masses indicate mass upper limits.  eV gives the upper limit on the sum of neutrino masses from cosmological observations (see text).

The Grand Unified Theory, GUT, is usually obtained assuming the absence of new physics between the electroweak scale and the GUT scale (1016 eV). The GUT scale cannot be reached with present or future accelerators. Several theorists consider intermediate energy scales and discuss possible new phenomenological effects [53].

If neutrinos have nonzero masses, the        are linear combinations of the      via the elements of the unitary mixing matrix , usually called the Pontecorvo-Maki-Nakagawa-Sakata (PMNS) mixing matrix: where the index in the summation is extended to the number of mass eigenstates. Neutrino oscillation experiments measure the probability of a flavor to convert into a after a time from production at some distance from the source. The corresponding probability can be expressed as where is the energy of the mass eigenstate . In vacuum, if CPT holds, .

For the neutrinos the mixing matrix is specified by three rotation angles, , , and , and three phases , , and   . In the conventional parameterization the matrix reads as follows: with , and similarly for the other sines and cosines , , . The action of the three rotation matrices is illustrated in Figure 2 with approximate values of the three mixing angles , , and , as presently known [49]. Neutrino oscillations depend on six independent parameters: two mass squared differences, and , three angles , , and , and the CP-violating phase . The (2-3) sector is identified with neutrino oscillations at the atmospheric scale and the (1-2) sector with oscillations at the solar scale; the (1-3) sector concerns and, for nuclear reactors, disappearance. The two phases, and , do not affect neutrino oscillations but may have physical consequences (e.g., in neutrino-less double beta decay) if neutrinos turn out to be Majorana particles.

464926.fig.002
Figure 2: Rotations between mass and flavor eigenstates in the 3 families neutrino oscillation scheme (, , and ).

In the approximation of two flavors (, ) and two mass eigenstates (, ) one can write In this case the oscillation probability (2) of a beam becomes where is the distance traveled by the neutrino from production to interaction in a detector and is the neutrino energy. The survival probability for the initial is .

In several cases one needs oscillations including three flavors [54].

Since neutrino oscillations are sensitive to (unsigned) neutrino mass differences (5) the present experimental data leave open two possibilities for mass ordering. Since (from solar matter effects measurements), there are two possibilities (normal mass hierarchy, ) or (inverted mass hierarchy, ).

In matter (e.g., inside the sun) CC coherent scattering of with atomic electrons changes the weak potential, a phenomenon known as the Wolfenstein-Mikheyev-Smirnov (MSW) effect [55, 56].

The oscillation parameters are modified according to where , with the electron density in matter and the Fermi constant.

We now recall the existing limits on neutrino masses, on the number of light neutrinos, and on neutrino lifetime obtained from searches at accelerators and from observational cosmology [4143, 57, 58].

Direct Measurements of Neutrino Masses. Many direct measurements were and are being performed using mainly tritium decay, , measuring, with magnetic spectrometers of ever increasing precision, the electron spectrum near its kinematical limit where the number of events is small, ~10−3 times of the whole sample. The present best limit is () < 2 eV (95% CL) [49]. Notice that in direct searches the upper limits correspond to a weighted average of the neutrino mass contributing to a given flavor since the measured quantity is

Limits on and masses were obtained at accelerators using muon and tau decays which yielded () 0.19 MeV, () < 18 MeV [49]. The last limit comes from the combination of results from different experiments, mainly at LEP. In these experiments the most sensitive conditions are when the decays into many charged pions [59].

Neutrino-less double- decay searches provide limits on the effective Majorana mass  . The present best upper limit ranges from 0.19 eV to 0.68 eV depending on the nuclear matrix calculation used [60]. It is worth noting that the discovery of the Majorana nature of neutrinos would have a deep impact on the general framework of the SM in which all fermions obey the Dirac equation: neutrinos would be the only exceptions.

Massive ’s and Cosmology. Massive stable neutrinos contribute to the overall energy density of the universe. In particular if 1 eV the neutrinos would affect the clustering of galaxies at relatively large cosmological scales. A limit on 0.3 eV was obtained by the Planck satellite collaboration [50].

Number of Light Neutrino Types. The most precise measurements of the number of light “active” neutrinos (i.e., neutrinos with electroweak couplings) come from the four LEP experiments. The combined result is [49].

The density of radiation in the universe, besides photons, is usually parametrized by the effective neutrino number . In the standard model of cosmology, .

The recent Planck observations provide no compelling evidence for additional neutrino species. Combining Planck, WMAP polarization, and the long baseline experiments gives (95% CL) [50, 61] Neutrino Lifetime. The indications from experiments and from cosmology are that neutrinos are either stable or long lived [62]. Specific experiments which searched for radiative solar neutrino decays during total solar eclipses yielded  s depending on the mass [63].

3. Atmospheric Neutrino Experiments

The main sources of atmospheric neutrinos are the decays of charged mesons ( and ) produced in the primary cosmic ray interactions with atmospheric atomic nuclei. Mesons in turn decay into and . At low energies muon decay gives rise to electron, electron neutrinos, and muon neutrinos: with fluxes and flux ratios . In this energy region the total atmospheric neutrino flux is of the order of 0.1 cm−2 s−1 and the energy spectrum can be approximated with a power law . The zenith angle distribution is asymmetric since at low energy the primary CR flux depends on the geomagnetic location and so does the neutrino flux.

At high energy muon decay can be neglected and meson decay remains the dominant atmospheric neutrino source. The neutrino flux steepens and it becomes asymptotically steeper than the primary flux . In this case the zenith angle distribution is symmetric around the horizontal direction where the neutrino flux is maximum since the path length in atmosphere is maximum and hence the probability of mesons to decay into neutrinos is symmetric.

Atmospheric neutrinos are well suited to study neutrino oscillations, since they have energies from a fraction of a GeV up to more than 100 GeV and they may travel distances from few tens of km up to 13000 km; thus the ratio in (5) ranges from 1 km/GeV to 105 km/GeV. In particular they cover regions for of the order of  eV2.

Atmospheric neutrino oscillations can be studied by means of three observables.(i)First, one can measure the ratio of the measured number of events over the predicted one. In order to reduce the systematic error related to the limited knowledge of the absolute flux normalization, one can use the double ratio in which the flux is referred to the flux.(ii)One may consider that there are two identical sources for a single detector: a near one (downgoing neutrinos) and a far one (upgoing neutrinos) which correspond, respectively, to a short and to a large baseline . For relatively high energy neutrinos ( GeV) the outgoing muon preserves with good accuracy the original neutrino direction and the path length can be measured. Assuming  eV2, from (5), for downgoing neutrinos and for upgoing neutrinos. Therefore the measurement of the flux ratio can directly provide information of the mixing angle .(iii)A third approach is to measure the flux reduction as a function of the baseline (and therefore of the zenith angle). In this case one may explore the argument of the second sinusoidal term in (5) (which was averaged to 1/2 in the previous case).

3.1. Early Experiments

The first experimental information on atmospheric neutrinos came in the 1960s and 1970s from two small detectors located at great depths in South Africa (KGF) [64] and in India (CWI) [65], then followed the experiments Baksan, IMB, Kamiokande, NUSEX, and Fréjus.

For all these studies the main motivation was the search for proton decay and atmospheric neutrinos were a background; only later the search for neutrino oscillations became an interesting possibility.

The Baksan Underground Scintillation Telescope is located at a depth of 850 m.w.e. in the Caucasus region. It is made of liquid scintillation counters placed to form a parallelepiped of 17 m 17 m 11 m. The selection of muon events produced by up-through-going neutrinos is made with time of flight methods. In the early data the zenith angle distribution deviated from expectations and seemed to agree with oscillations [30]. Later they considered also the absolute number of events and there is an agreement with Monte Carlo predictions; the ratio data/MC is 1.00 0.04 (stat.) 0.08 (syst.) [31].

The IMB detector was an 8000 t cylindrical water box placed in the Morton salt mine in Ohio, 1750 m.w.e. deep underground [22, 23]. The Cherenkov light produced by relativistic charged particles passing in the water was detected by photomultipliers installed in the tank walls. The detector started operation in 1982 and was upgraded by increasing the size of the photomultipliers.

The Kamiokande cylindrical detector had a water mass of 3000 t seen by 1000 large PMTs of 50 cm diameter [2426, 49]. It was installed in the Kamioka mine in Japan at a depth of 2700 m.w.e. It started operations in 1983 and had several upgrades, known as Kamiokande I, II, and III.

The NUSEX detector was a fine granularity detector with a total mass of 150 t, placed in the Mont Blanc tunnel between Italy and France at a depth of 4800 m.w.e. The detector was made of horizontal 3 mm iron plates interleaved with layers of limited streamer tubes [27].

At the same depth was located the 912 t Fréjus detector. It was made of pairs of vertical iron slabs each 1.5 mm thick interleaved with pairs of planes of flash tubes; their trigger was made with Geiger tube layers inserted every 8 layers of flash tubes [28, 29].

The early water Cherenkov detectors and the tracking calorimeters detected and charged current interactions. The results were expressed in terms of the double ratio , where = is the ratio of observed muon and electron events and is the same ratio for Monte Carlo (MC) events. In many systematic uncertainties cancel. The double ratios from IMB and Kamiokande were smaller than expectations, while for NUSEX and Fréjus they were in agreement with expectations without oscillations. The IMB collaboration concluded that “however the magnitude of the deviation is not sufficient to require neutrino oscillations to explain our data.” The overall spectra and total number of interactions were in agreement with predictions. Furthermore there was no correlation of deficit with energy or angle [22, 23]. The Kamiokande experiment obtained indications for oscillations with maximal mixing and  eV2, a value considerably larger than the present best value  eV2 [2426].

3.2. The Discovery of Atmospheric Neutrino Oscillations

At the Neutrino 1998 Conference, Soudan-2, MACRO, and Super-Kamiokande (SK) presented strong indications in favor of atmospheric neutrino oscillations [3338]. After 1998 several additional results were presented [6670].

The Soudan-2 experiment [69, 70] used a modular fine grained tracking and showering calorimeter of 963 t, located at a depth of 2100 m.w.e. in the Soudan Gold mine in Minnesota. The bulk of the target was 1.6 mm thick corrugated steel sheets interleaved with drift tubes. In the final analysis fully contained high resolution events, consisting mostly of quasi-elastic neutrino interactions were used. The data were compared with the Bartol Monte Carlo neutrino flux [39]. The double ratio = integrated over the zenith angle was (0.68 0.11), consistent with oscillations with maximal mixing and = 5.2 × 10−3 eV2(Figure 6(b)). The experiment ended in 2001.

The MACRO experiment operated at the Gran Sasso underground Lab (3800 m.w.e.) from 1989 to 2000. Figure 3 shows a global view and a cross section of the detector. It used 3 different subdetectors: scintillation counters, limited streamer tubes, and nuclear track detectors [71]. Up-through-going muons with  GeV came from CC interactions in the rock below the detector and had  GeV. The angular distribution of these muons is highly sensitive to neutrino oscillations as can be seen in Figure 4.

fig3
Figure 3: Cross section (a) and global view (b) of the MACRO detector. In the left figure are also shown the observed neutrino-induced event topologies.
464926.fig.004
Figure 4: Reduction factor in the number of upgoing muons for different values for a muon detection threshold of 1 GeV (MC studies). Note the shape dependence vs the values.

The MC scale uncertainties on the expected muon flux arising from the neutrino flux, cross section, and muon propagation were estimated at 17%. In Figure 5(a) the zenith angle distribution is compared with MC predictions. A measurement of the up-through-going muon energies was made via multiple Coulomb scattering in the dense structure of the apparatus using the streamer tubes in “drift mode” [72, 73]. The ratios Data/ as a function of give additional information on neutrino oscillations.

fig5
Figure 5: (a) MACRO up-through-going muons compared with oscillated and nonoscillated predictions of different MCs [68]. (b) Measured zenith distributions for the IU low energy events. The black points are data; the shaded region is the MC predictions with no oscillations. The full line is for oscillations with maximal mixing and  eV2.
fig6
Figure 6: (a) The MACRO ratio between the data in two angular bins (black point on gray line) and comparison with MC oscillations. (b) 90% CL allowed regions for the oscillations up to year 2004.

Low energy neutrino events 2-3 GeV (Figure 5(b)) included (i) semicontained upgoing muons (IU) from interactions inside the lower part of the apparatus, (ii) upgoing muons stopping in the detector (UGS) due to external interactions, and (iii) semicontained downgoing muons (ID) originating from interactions in the lower detector. The lack of time information prevented distinguishing between ID and UGS samples. In Figure 5(b) the number of IU events and the angular distributions are compared with MC predictions. The data show a uniform deficit over the whole angular distribution with respect to MC.

In 1998 MACRO results were consistent with neutrino oscillations, with = 2.5 × 10−3 eV2 and maximal mixing [3437]. In the final analysis [68] three different ratios were considered in order to reduce systematic uncertainties and MC prediction effects: the ratio of vertical over horizontal neutrino events in the up-through-going data sample; the ratio of low energy over high energy neutrino events; the double ratio for the semicontained data sample. Fitting the three ratios to the oscillation hypothesis MACRO obtained and  eV2. In Figure 6(b) the 90% CL allowed parameter region is shown. The addition of the absolute flux information in the global fit increased the statistical significance of the result to the level.

Since and interactions with matter share the same weak potential whereas sterile neutrinos do not experience weak interactions, a possibility to discriminate between and oscillations is to study the neutrino flux emerging from different matter amounts. That was realized by comparing events near the vertical direction with the event number near the horizontal direction [74, 75]. The angular regions were chosen by MC methods to obtain the best discrimination (Figure 6(a)). In the ratio most of the uncertainties cancel. MACRO excluded at the 99.8% CL the oscillations compared to the channel [76].

The Super-Kamiokande (SK) detector is a large cylindrical water Cherenkov detector containing 50 kt of water, with a fiducial mass of 22.5 kt. The experiment is still taking data. The Cherenkov light is seen by 50 cm diameter inner-facing phototubes (PMTs) (Figure 7). The 2 m thick outer layer of water acts as an anticoincidence using smaller outward facing PMTs. The detector is located in the Kamioka mine, Japan. The experiment was originally planned mainly to search for proton decay. Atmospheric neutrinos are detected through the Cherenkov light generated by the charged particles produced in neutrino CC interactions in the water. The large detector mass allows defining a fiducial volume large enough to collect good samples of fully contained events (FC) up to 5 GeV. The events are further subdivided into sub-GeV and multi-GeV events, with energies below and above 1.33 GeV. The partially contained events (PC) are CC interactions where the vertex is within the fiducial volume and a charged particle, a muon, exits the detector without releasing all of its energy (Figure 8). In this case the light pattern is a filled circle. For these events the energy resolution is worse than that for FC interactions. Upward-going muons (UPMU), produced by upgoing neutrinos coming from interactions in the rock, are subdivided into stopping muons ( GeV) and up-through-going muons (with  GeV) if they stop or not in the detector.

464926.fig.007
Figure 7: Global view of the SK detector.
464926.fig.008
Figure 8: Zenith angle distributions from the SK detector (data from SK I + SK II + SK III) [77].

Particle identification in SK is performed using likelihood functions to parameterize the sharpness of the Cherenkov rings, which are more diffuse for electrons than for muons. The algorithms discriminate the two flavors with high purity. The zenith angle distributions for -like and -like sub-GeV and multi-GeV events, for PC events and upward-going or stopping muons, are shown in Figure 8.

At the time of Neutrino '98 Conference the values for the double ratio previously defined were for the sub-GeV sample and for multi-GeV [66, 67].

SK uses a selected sample of events with good resolution in to search for the dip in the oscillation pattern expected when the argument of the second sine-squared term in (5) is . The dip is observed at  km/GeV (Figure 9). These results favor oscillations and provide a further constraint on . Other models that could explain the zenith angle and energy dependent deficit of the atmospheric muon neutrinos are disfavored since they do not predict any dip in the distribution. For oscillations the best fit yields maximal mixing and = 2.3 × 10−3 eV2 [66, 67].

464926.fig.009
Figure 9: Data/MC ratio versus (black points) for SK. The red solid line is the MC expectation with = 2.5  eV2 and maximal mixing [66, 67].

Several tests were performed by the SK experimenters and by several groups of phenomenologists on the possibility [78], on the possible LVI [79, 80], and so forth. SK made also a variety of fits of the SK I, II III, and IV data sets in the 3-flavor oscillation scenario obtained at 90% CL:  eV2 and . In the 3-flavor analysis there is no preference for normal or inverted neutrino mass hierarchy [78, 81].

SK also searches for appearance studying several event-related variables with a neural network. Despite the complicated event topology and the high background they claimed a 2.4 significance [82], recently updated with SK I + II + III data to 3.8.

Super-Kamiokande has the largest statistics in different energy regions, all in agreement with atmospheric oscillations. The SK main results are summarized in Table 2 and Figures 8, 9, 10, and 11(b). With more data and a 3-flavor analysis SK may be able to find if is smaller than its maximum and to determine in which octant it lies [83, 84].

fig10
Figure 10: (a) Reconstructed energy spectrum for 58 one-ring events detected by K2K. The dashed blue line is for MC no oscillations; solid red line is the MC oscillation best fit. Both MC histograms are normalized to the data. (b) Comparison of K2K results with the SK atmospheric neutrino measurement [102, 103].
fig11
Figure 11: (a) Photograph of the MINOS far detector: “A” indicates the magnetized iron sheets, “C” is the electric coil, and “B” is an anticoincidence scintillator system. (b) versus for oscillations measured by MINOS [104] and other experiments [105].

Several proposals were made for the Gran Sasso Lab, for example, the MONOLITH proposal for a massive magnetized iron detector for atmospheric neutrinos [85]. For the future there should be the INO proposal for an India-based Neutrino Observatory [86].

4. The Mixing Angle

In the limit , atmospheric and solar neutrino oscillations decouple and can be analyzed separately in the 2-neutrino-flavor approximation.

The knowledge of is very important since it is strictly connected with the CP-violating phase in the matrix element, . Its precise knowledge is decisive for further experiments.

The first two experiments at nuclear reactors, which attempted to measure in disappearance mode, were CHOOZ and Palo Verde [87, 88]. No evidence for disappearance was found. They obtained limits for at the level of for .

Recently 3 experiments, Daya Bay, Double Chooz, and RENO, each using several nuclear reactors, measured the neutrino oscillation angle , the last parameter needed to really understand the phenomenon of neutrino oscillations. The nuclear reactors are of the latest French-German design (EPR of generation 3 or ) [8995]. In Table 1 the most relevant parameters of neutrino reactor experiments are given:(i)6 reactors in China (Exp. Daya Bay): [8991],(ii)2 reactors in France (Exp. Double Chooz): [92, 93],(iii)6 reactors in Republic of Korea (Exp. Reno): [94, 95].

tab1
Table 1: Nuclear reactor experiments Daya Bay, Reno, and Double Chooz. For each experiment the location, the number of nuclear reactors, the overall thermal power, the near/far detector distances, and the approximate depth of near/far detectors are given. Note that Daya Bay has two separate reactor core sites and therefore two near/far distances.
tab2
Table 2: Main parameters and results of some relevant atmospheric neutrino experiments.

These experiments used refined detectors. They obtained important results taking advantage of the very large fluxes of low energy from the power reactors. was found to be small but not zero: the average value is [49]. T2K confirmed the measurement [96]. The measured value of opens the possibility of performing many types of precision measurements in the leptonic sector [97101].

5. Long Baseline High Energy Oscillation Experiments

Long baseline accelerator experiments provide independent measurements of oscillation parameters. Some of these experiments may be complementary to reactor experiments. By combining the results of two such experiments at different baselines, the sign of could be determined.

High energy neutrino beams are produced accelerating protons up to tens of GeV and impinging them on a target. The produced secondaries are momentum-selected by a series of lensing devices (“horns”) which focus them into a parallel beam in an evacuated decay tunnel of 1 km length. Table 2 summarizes the main parameters of atmospheric experiments. In Table 3 the main parameters of past, present, and possible future long-baseline neutrino oscillation experiments are listed.

tab3
Table 3: Main parameters of past, present, and future long-baseline neutrino oscillation experiments.

The K2K experiment confirmed the atmospheric muon neutrino oscillation picture [102, 103]. Near detectors located at 300 m from the target measured the energy spectrum and the flux normalization. In total 112 beam-originated neutrino events were observed in the SK fiducial volume with an expectation of events for no oscillations, providing a statistical significance against no oscillations of 4.3. A subsample of 58 one-ring events was assumed to be quasi-elastic interactions and energy reconstructed using the known beam direction. The energy spectrum in Figure 10(a) shows the energy-dependent distortion expected from oscillations. In a 2-flavor oscillation scenario, the best-fit value yielded =  eV2 and maximal mixing. The K2K allowed region for the oscillation parameters is consistent with that from atmospheric neutrino data (Figure 10(b)).

The NuMi 3.7 GeV energy neutrino beam uses neutrinos produced by the Fermilab Main Injector, a 120 GeV proton synchrotron capable of accelerating protons with a cycle time of 1.9 s. The flavor composition of the beam is 98.7% (), with a relatively large fraction of .

MINOS on the NuMi beam uses a near detector at Fermilab and a far detector at the Soudan mine site, 735 km away, at a depth of 2090 m.w.e. Both are iron-scintillator sandwich calorimeters with a toroidal magnetic field in the octogonal iron plates, interleaved with active planes of long scintillator strips providing both calorimetric and tracking information. The far detector (Figure 11(b)) has a total mass of 5400 t. The magnetic field is 1.3 T. The near detector, with a total mass of 920 tons, is installed 250 m downstream from the end of the decay pipe.

MINOS confirmed the atmospheric neutrino oscillation picture with improved accuracy in , not in angle (Figure 11(a)). It rejects neutrino decay [106] and decoherence [107]. In the scheme it obtains  eV2 and (90% CL) [104, 108, 109].

The CERN to Gran Sasso Neutrino Beam (CNGS). The 400 GeV proton beam from the CERN-SPS is transported to an underground target. Secondary pions and kaons are focused into a parallel beam and decay into and . The remaining hadrons are absorbed in the hadron stopper. The muons are monitored by two silicon detectors. The mean energy is 17 GeV. The muon beam size at the second muon detector at CERN is 1 m; the beam size at Gran Sasso is 1 km. Figure 12 shows the 730 km path of the beam from CERN to the Gran Sasso Lab (LNGS). It also indicates the synchronization via GPS of the atomic clocks at CERN and at LNGS. The CNGS beam was conceived to study the oscillation phenomenon in appearance mode; the spectrum was tuned to maximize the lepton production above its 3.5 GeV kinematic threshold.

464926.fig.0012
Figure 12: Sketch of the 730 km neutrino path from CERN to Gran Sasso and the GPS selection of events.

During the 90s the appearance was searched for in the “cosmologically relevant region”  eV2 by two short-baseline experiments, CHORUS  [110] and NOMAD [111], which relied on different techniques to search for appearance. Both experiments excluded oscillations for  eV2.

OPERA at LNGS is a hybrid emulsion-electronic detector (Figure 13), designed to search the appearance in the CNGS beam [112115], in the parameter region indicated by the atmospheric neutrino experiments. The appearance search is based on the detection of the lepton in nuclear emulsions. The 1.25 kt target is segmented in units (bricks) consisting of 56 lead plates (1 mm thick) and 57 emulsion layers; each brick weighs 8.3 kg. Events may be analyzed in the electronic detector and/or in the emulsions. Fast automated scanning systems running at 20 cm2/h per emulsion layer were developed to cope with the emulsion analysis load [112121]. In a brick the spatial and angular resolutions are 1 m and 2 mrad.

464926.fig.0013
Figure 13: Schematic of the OPERA experiment in Hall C at Gran Sasso.

So far OPERA found three candidate events (Figure 14) [122124]. In Figure 14(a) tracks 1–6 originate from the primary interaction vertex, and track 7 is a prompt neutral particle, and track 4 has a kink topology compatible with a -lepton decay. and in Figure 14(b) are -rays from the secondary vertex; their invariant total mass is compatible with decay. Track 8 is from a . The invariant mass of the and of the is compatible with that of (770) mass. The decay of the short track is thus compatible with . The second and third event are shown in Figures 14(b) and 14(c). From these results the evidence for appearance can be established at the level [123, 124]. The analysis of events is ongoing; the final result of appearance search is expected by the end of 2014.

fig14
Figure 14: Display of three candidate events from the OPERA experiment. (a) First event , , (b) second event , , and (c) third event , .

The OPERA search for limited the window region for the LSND anomaly [125].

OPERA made a measurement of the velocity and, after solving some technical problems, obtained precision measurements with the normal beam and with a special “bunched beam” [125128].

The ICARUS T600 detector is an innovative TPC liquid argon detector which ran on the CNGS beam, in Hall B of LNGS. One event recorded by T600 is shown in Figure 15. ICARUS performed a search for to limiting the window of open options for the LSND anomaly [129, 130].

464926.fig.0015
Figure 15: One CNGS event recorded in the ICARUS T600 detector.

The T2K (from Tokai to Kamioka) experiment is a second generation long baseline experiment, which uses a 2.5° off-axis neutrino beam produced by 30 GeV protons at the Japan Proton Accelerator Research Complex (J-PARC) [131]. The neutrino beam is sent to the SK detector, 295 km away; because of the kinematics of pion decay it emerges as a narrow beam peaked at 600 MeV. The schematic view of the neutrino beam line is sketched in Figure 16(a). A sophisticated near detector complex (ND280) was built at a distance of 280 m from the target. It includes the on-axis monitor INGRID and an off-axis detector, a spectrometer with a magnetic field of 0.2 T which includes a detector, a projection chamber system, two scintillation detectors, a electromagnetic calorimeter, and a muon range detector. A single -like beam event detected in the SK detector is shown in Figure 16(b). 28 candidate events were detected and compared to an expected background of events. The excess events at SK correspond to a confidence interval of for normal hierarchy [132135], and now it has a 7.5 significance for [96].

fig16
Figure 16: Sketch (a) of the T2K beam line, showing the primary proton beam line, the target station, the decay volume, the beam dump, the muon monitors, and the near on-axis and off-axis neutrino detectors. On (b) a single ring event in the SK detector.

The NOA experiment, which will run using an upgraded NuMI beam, is in an advanced construction phase. A proton beam power of 0.7 MW is planned, with  GeV and a baseline of 810 km, 14 mrad off-axis. The detector will be a 15 kt “totally active” tracking liquid scintillator, scheduled to be partly operational by the end of 2013. It will be placed at ground level in Northern Minnesota. The close detector will be a 220 t replica of the far detector, placed 14 mrad off-axis at ~1 km from the target. The main NOA physics aims include the study of disappearance and appearance with a precision about one order of magnitude better than at present [136].

5.1. The LSND Scale

In the 90s at the Los Alamos Laboratory in New Mexico the 800 MeV proton linear accelerator was used to produce a beam with energies up to 300 MeV (from muon decays at rest) incident on the Liquid Scintillator Neutrino Detector (LSND), designed primarily to search for oscillations. A 3.8 sigma excess of candidate events was observed and interpreted as due to neutrino oscillations with a small mixing angle and a relatively large in the 0.2–10 eV2 range [137, 138]. The results do not fit in the conventional 3 neutrino mixing scheme and require at least a fourth neutrino (sterile neutrino).

The KARMEN [139] reactor experiment partly ruled out the LSND results leaving a small region, 0.2–2 eV2, still compatible with the LSND oscillation signal.

The MiniBooNE experiment was designed to provide a test of the LSND signal. It used the Fermilab Booster neutrino beam generated from 8 GeV protons incident on a Be target. The center of MiniBooNE was 541 m from the production target. The near neutrino target was mineral oil in which relativistic particles created both Cherenkov and scintillation light. The experiment did not confirm the LSND results but found an excess of electron-like events in the neutrino energy range below 475 MeV [140]. The source of the excess remains unexplained, although several hypotheses were put forward [141, 142]. MiniBooNE reported on an updated search in antineutrino mode: an excess of events for energies above 475 MeV was observed. The fit allowed regions for oscillations in the 0.1 to 1 eV2 range are consistent with the allowed region reported by LSND.

The search for sterile neutrinos is very active. The SM already provides right-handed neutrinos, which are “sterile” with respect to gauge bosons of the electroweak sector. Experimental searches concern light sterile neutrinos ( eV), which could mix with active neutrinos and oscillate at short baselines.

In addition to the LSND and MiniBooNE results, which involve electron (anti)neutrino appearance in , beams, other anomalies in disappearance mode were found to fit the same sterile neutrino scenario at the eV scale. The so-called “gallium anomaly” refers to the deficit in radioactive source calibration tests, at the gallium solar neutrino experiments SAGE and GALLEX [143]. A reevaluation of flux from reactors exceeded the measured value by 6% (“reactor anomaly”) [144]. A recent reanalysis stresses that uncertainties may be larger than the anomaly [145]. When interpreted in terms of active to sterile neutrino oscillations, both gallium and reactor anomalies lead to oscillation parameters compatible with LSND and MiniBooNE results. It should be noted that the no-oscillation hypothesis is rejected at about 6, even if most of the statistical power is driven by LSND: removing LSND from the analysis, the oscillation significance drops to about 2 [146]. Moreover it was found that the disappearance channel is compatible with no oscillations in contradiction to what is expected, thus generating a tension with respect to previous results. The disappearance channel in this region will be explored using atmospheric neutrinos in large acceptance detectors such as neutrino telescopes [147]. In the near future the SOX experiment will test the reactor and gallium anomalies by detecting neutrinos and antineutrinos from MCi sources, with Borexino [148].

Among the various ideas to tackle the sterile neutrino problem the SPSC-P-347 proposal (ICARUS-NESSiE) at CERN would be a complete experimental setup to solve this issue. The project would exploit the ICARUS T600 detector as a far detector in a new low energy beam line at the CERN SPS. In addition a 150 t LAr detector clone could be placed at 460 m from the target position to provide the unoscillated pattern. Two magnetic spectrometers would be placed downstream of the two LAr-TPC detectors to complement and enlarge the physics reach of the experiment. The LAr-TPC technology allows identifying and reconstructing interactions. Muon neutrinos could be also identified even if charge reconstruction would be performed only at a statistical level with a large discrimination power. The spectrometers could complement and improve the muon neutrino sector by extending the measurable spectrum and performing charge identification at the 1% level on an event-by-event basis. The ICARUS-NESSiE proposal could span a large fraction of the parameter space in a limited time window simultaneously facing the appearance and disappearance channels and also providing a measurement of NC rates which are considered reliable signals of sterile neutrino existence [149152].

6. Neutrino Oscillations and New Physics

Mechanisms other than flavor transitions have been tested as alternative or subdominant processes to explain atmospheric data (i.e., violation of the equivalence principle, of Lorentz invariance, and of CPT symmetry) [153]. The most relevant feature of these scenarios is the departure of the energy dependence of the oscillation length.

Lorentz Invariance Violation (LIV). MACRO and SK up-through-going muon data were used to search for subdominant oscillations due to a possible LIV: in this case there could be mixing between flavor and velocity eigenstates. Limits were placed in the Lorentz violation parameter at = 0 and at = 1 [154]. In the context of a Standard Model Extension (SME) quantum strings could introduce nonlocality that could break Lorentz and/or CPT invariance. The neutrino oscillation probability may depend on the direction of the neutrino propagation; this effect would manifest, in experiments with both neutrino source and detector fixed on Earth, as a sidereal modulation in the number of detected neutrinos. This was searched for by the MINOS near detector without finding any effect: in the context of SME one could set limits on the magnitude of the Lorentz and CPT violating terms at the level of of the maximum expected, assuming a suppression of the signature by a factor of [155]. More stringent limits may be obtained by neutrino telescopes; see Section 8.

Neutrino Decay. Using SK data Fogli et al. [79, 80] have shown that the neutrino decay hypothesis fails to reproduce the observed zenith angle distribution of atmospheric neutrinos. MINOS excluded neutrino decay at 7 standard deviations studying the distribution [104].

The radiative decay modes allowed for massive neutrinos are and [62]. A direct experimental limit comes from the 2006 total solar eclipse in the Libya Sahara desert [63]. For the radiative decay the 95% CL lower lifetime limits are in the range 10 s  s for neutrino masses  eV  eV [63]. A similar limit was obtained for the decay, but the limit is tentative since it depends on the mixing angle which was not known at that time.

Extra Dimensions. In models where the standard dimensional world (“brane”) is embedded in a larger dimensional spacetime (“bulk”)—with being the number of extra dimensions—and SM left-handed neutrinos are frozen within the brane while right-handed neutrino singlets can propagate in the bulk. They give rise to perturbations that can alter the “standard” oscillation pattern of active neutrinos. By combining the results from KamLAND and MINOS a limit 1 μm was obtained on the size of the larger hidden dimension [156].

Lepton Flavor Violation. Neutrino oscillations arise from flavor mixing in the leptonic sector. In the SM the violation would be minimal and lead to a very small branching ratios for processes which violate lepton flavor, like decay. Supersymmetric (SUSY) theories could give rise to lepton flavor violations through radiative corrections which could increase the branching ratio. This could happen also for electric dipole moments, for example, of the neutron and of the muon. The MEG collaboration published limits on the search for decay: < (90% CL) [157].

7. Cross Section and Particle Production Measurements

After 1998 it was realized that the existing measurements of hadron production concerned mainly very forward angles and high momenta and were not adequate for the proper atmospheric neutrino simulations and for conventional and advanced neutrino beams. In 2000 the HARP experiment at the CERN-SPS pioneered systematic hadron production measurements over the full acceptance in angle and in momentum. It used proton and pion beams on different target materials [158]. It produced the pion data needed for the K2K and MiniBooNE experiments.

New neutrino cross-section measurements were also made by the K2K near detector (~1.2 GeV), MiniBooNE (~800 MeV), SciBooNE (~800 MeV) [159, 160], MIPP (from 1 to 120 GeV), NA61/SHINE experiment at the CERN-SPS [161, 162], and T2K [163].

The MINERvA experiment in the NuMI beam-line at Fermilab is a fine-grained detector which will provide neutrino scattering data in the ~1–20 GeV region [164167].

8. Neutrino Telescopes and Atmospheric Neutrinos

Large size neutrino telescopes were built mainly to shed light on the most violent and energetic phenomena in the universe using high energy neutrinos as astrophysical probes. High energy neutrinos with hundreds of GeV may come from nonthermal astrophysical sources [168]. Multi-GeV neutrinos may also come from the interior of celestial bodies, like the sun, some planets, and the center of our galaxy where annihilation of weakly interactive massive particles (WIMPs) could take place. These searches require large detectors, like the Baikal detector in lake water [169], Amanda [170] and IceCube [171173] in South Pole ice, and ANTARES in the Mediterranean sea [174176]; a multi-km3 detector is planned for the Mediterranean sea (Km3NeT) [177]. The observation of neutrinos is based on the Cherenkov light induced by upgoing muons produced in high energy CC interactions (to reduce the background from atmospheric muons, neutrino telescopes look downward). Large arrays of PMTs cover huge volumes of ice or sea water.

The cosmic very high energy neutrino flux is expected to decrease with energy as . Atmospheric neutrinos are a background with an energy dependence of . The possibility to perform neutrino oscillation studies is related to the energy threshold for detecting lower energy atmospheric neutrinos. If the spacing between neutrino telescope strings is reduced (as in the IceCube Deep Core array), the energy threshold is ~20 GeV. It could be as low as few GeV in the future Km3NeT-ORCA and IceCube-PINGU inner cores. This opens the possibility to perform high statistics oscillation analyses up to ~1 TeV, above which the Earth starts to become opaque to neutrinos. The IceCube present Inner Core allowed a first measurement of the atmospheric oscillations which yielded in a 2- flavor formalism: and . The no-oscillation hypothesis is rejected [178181]. The ANTARES experiment obtained a measurement of of limited accuracy, , but it checks the status of the apparatus and underlines the potential for future physics [174176].

Figure 17 shows the atmospheric energy spectrum in the range 0.1–400 TeV, measured by the IceCube, ANTARES, and AMANDA-II neutrino telescopes, using different energy estimators and different unfolding methods. The data are compared with the MC Bartol flux and with the more elaborate Bartol + Martin, Bartol + Enberg calculations. Within large systematic errors, the results from different experiments are compatible with each other and with the theoretical MC predictions [182184]. The data do not confirm nor reject the presence of prompt components.

464926.fig.0017
Figure 17: Atmospheric muon neutrino spectrum in the 0.1–200 TeV energy range, measured by ANTARES, AMANDA-II, and IceCube compared with the Bartol, Bartol + Martin, and Bartol + Enberg MC fluxes.

Neutrino telescopes have searched for Lorentz invariance violations. IceCube, operating in a 40-string configuration, searched for a periodic variation in right ascension, a possible consequence of LIV preferred frame. No such direction-dependent variation was found, and, due to the unique high energy reach of IceCube, it was possible to improve constraints on certain LIV oscillation by about three orders of magnitude with respect to other experiments [178181].

Very large neutrino telescopes could also yield more precise direct and indirect results on dark matter (WIMPs) and on the searches for various exotic particles.

9. Conclusions and Perspectives

The standard model of particle physics obtained important confirmations in all experiments at LEP, SLC (), HERA (), and Fermilab () colliders, and a Higgs boson-like particle has been seen at the CERN LHC, but the SM needs further confirmations.

Neutrino oscillations provided a first indication for physics beyond the standard model. The atmospheric neutrino anomaly was experimentally observed and explained as due to neutrino oscillations with maximal mixing and  eV2. It was later confirmed with more data and by the long baseline neutrino experiments, including appearance experiments () with direct detection in nuclear emulsions.

It may be interesting to consider the variations with time of the atmospheric oscillation parameters published by different experiments. In the two neutrino scenario, , most experiments obtained maximal mixing and values of which changed only slightly with time (in units of  eV2):(i)in 1998: 2.3 (SK), 2.5 (MACRO), and 5.2 (Soudan-2),(ii)in 2004: 2.5 (SK), 2.3 (MACRO),(iii)in 2006: 2.8 (K2K),(iv)in 2008: (MINOS),(v)in 2010: (MINOS), 2.2-2.3 (SK 2-flavor; 2.11 and 2.51 SK 3-flavor analyses for normal and inverted hierarchy, resp. [81]),(vi)in 2013: (MINOS), , 2.44 (T2K), , (IceCube DeepCore), and , (ANTARES).

Globally the variations and the differences among the values from different experiments are small and well within their systematic errors. The variations are negligible compared to those reported in the early experiments on weak interactions and early atmospheric experiments.

In the three-active-neutrino frameworks one would like to solve the so-called “eightfold” degeneracy. Assuming the measured value of and running in mode there are two different sets of parameters (, ) producing the same oscillation probabilities. These “clone solutions” are doubled by the unknown sign of (normal or inverted hierarchy) and redoubled by the octant degeneracy, that is, the sign of . The problem may be solved by performing complete 3 neutrino analyses and by considering combinations of different baselines and energies [185, 186].

Several groups worldwide are investigating future neutrino beams of higher intensity and purity: superbeams, beta-beams, and neutrino factories [187, 188]. High intensity beams (superbeams) from high intensity proton accelerators are based on the improvements of existing proton accelerator complexes. Beta-beams could be produced from radioactive ion beams, taking advantage of the technological progress in this field. The beta decays of unstable ions would lead to pure sources of and beams, which could be used to study oscillations. High energy muon colliders have been studied for several purposes, in particular to obtain electron and muon neutrino beams from muon decays. The goal is to make high energy and high intensity muon storage rings which could be used as neutrino factories. It was proposed that simultaneous and decays could lead to important tests of CP violation in the leptonic sector [186, 188, 189].

The recent measurements of , together with the plans for upgraded higher intensity neutrino beams and new large refined detectors, open the door to a new golden age for neutrino physics, where one could obtain important information on neutrino masses and neutrino hierarchy, establish if is maximal or, if it is not, in which octant it lies, and make important tests of CP violation in the leptonic sector.

New large neutrino telescopes may improve the knowledge on dark matter, on supernovae neutrinos, and on the measurements of some parameters of atmospheric neutrino oscillations. Do sterile neutrinos exist? Are sterile neutrinos the explanation of existing experimental data which cannot be reconciled with the standard mixing scenario?

The search for new physics beyond the SM will be one of the main fields of research at the LHC. Supersymmetry is still one of the theoretically favored models and this could shed light on dark matter. Other topics such as compositeness, technicolor, and extra dimensions could be searched for at the new energy frontier. LHC may also yield information on neutrinos [190].

Acknowledgments

The authors acknowledge many discussions and the cooperation of many colleagues in Bologna, at the Gran Sasso Lab, and at CERN. They thank Drs. S. Balestra, S. Biagi, M. Errico, L. A. Fusco, N. Mauri, M. Pozzato, Z. Sahnoun, and V. Togo for their technical cooperation.

References

  1. B. Pontecorvo, “Mesonium and anti-mesonium,” Soviet Physics. JETP, vol. 6, p. 429, 1957. View at Google Scholar
  2. B. Pontecorvo, “Inverse beta processes and non conservation of lepton charge,” Soviet Physics. JETP, vol. 7, p. 172, 1958. View at Google Scholar
  3. Z. Maki, M. Nakagawa, and S. Sakata, “Remarks on the unified model of elementary particles,” Progress of Theoretical Physics, vol. 28, no. 5, pp. 870–880, 1962. View at Publisher · View at Google Scholar · View at Zentralblatt MATH
  4. B. Pontecorvo, “Neutrino experiments and the problem of conservation of leptonic charge,” Soviet Physics. JETP, vol. 26, p. 984, 1968. View at Google Scholar
  5. R. Davis Jr., D. S. Harmer, and K. C. Hoffman, “Search for neutrinos from the sun,” Physical Review Letters, vol. 20, no. 21, pp. 1205–1209, 1968. View at Publisher · View at Google Scholar · View at Scopus
  6. B. T. Cleveland, T. Daily, R. Davis Jr. et al., “Measurement of the solar electron neutrino flux with the homestake chlorine detector,” Astrophysical Journal Letters, vol. 496, no. 1, pp. 505–526, 1998. View at Publisher · View at Google Scholar · View at Scopus
  7. J. N. Bahcall, “Solar neutrinos. I. theoretical,” Physical Review Letters, vol. 12, no. 11, pp. 300–302, 1964. View at Publisher · View at Google Scholar · View at Scopus
  8. J. N. Bahcall and R. Davis, “On the problem of detecting solar neutrinos,” BNL-8217, 1964.
  9. J. N. Bahcall, P. I. Krastev, and A. Y. Smirnov, “Where do we stand with solar neutrino oscillations?” Physical Review D, vol. 58, no. 9, Article ID 096016, 1998. View at Google Scholar · View at Scopus
  10. J. N. Bahcall, W. A. Fowler, I. Iben, and R. L. Sears, “Solar neutrino flux,” The Astrophysical Journal, vol. 137, p. 344, 1963. View at Publisher · View at Google Scholar
  11. P. Anselmann, W. Hampel, G. Heusser et al., “GALLEX results from the first 30 solar neutrino runs,” Physics Letters B, vol. 327, no. 3-4, pp. 377–385, 1994. View at Publisher · View at Google Scholar · View at Scopus
  12. J. N. Abdurashitov, V. N. Gavrin, S. V. Girin et al., “Measurement of the solar neutrino capture rate with gallium metal,” Physical Review C, vol. 60, no. 5, Article ID 055801, 32 pages, 1999. View at Publisher · View at Google Scholar
  13. J. N. Abdurashitov, E. L. Faizova, V. N. Gavrin et al., “Results from SAGE-The Russian-American gallium solar neutrino experiment,” Physics Letters B, vol. 328, no. 1-2, pp. 234–248, 1994. View at Publisher · View at Google Scholar
  14. M. Altmann, M. Balata, P. Belli et al., “Complete results for five years of GNO solar neutrino observations,” Physics Letters B, vol. 616, no. 3-4, pp. 174–190, 2005. View at Publisher · View at Google Scholar · View at Scopus
  15. K. S. Hirata, T. Kajita, T. Kifune et al., “Observation of 8B solar neutrinos in the Kamiokande-II detector,” Physical Review Letters, vol. 63, no. 1, 16 pages, 1989. View at Publisher · View at Google Scholar
  16. K. S. Hirata, K. Inoue, T. Kajita et al., “Results from one thousand days of real-time, directional solar-neutrino data,” Physical Review Letters, vol. 65, no. 11, pp. 1297–1300, 1990. View at Publisher · View at Google Scholar · View at Scopus
  17. Q. R. Ahmad et al., “Measurement of the rate of νe+dp+p+e interactions produced by 8B solar neutrinos at the Sudbury Neutrino Observatory,” Physical Review Letters, vol. 87, no. 7, Article ID 071301, 6 pages, 2001. View at Publisher · View at Google Scholar
  18. Q. R. Ahmad, R. C. Allen, T. C. Andersen et al., “Direct evidence for neutrino flavor transformation from neutral-current interactions in the Sudbury Neutrino Observatory,” Physical Review Letters, vol. 89, no. 1, Article ID 011301, 6 pages, 2002. View at Publisher · View at Google Scholar
  19. K. Eguchi, S. Enomoto, K. Furuno et al., “First results from KamLAND: evidence for reactor antineutrino disappearance,” Physical Review Letters, vol. 90, no. 2, Article ID 021802, 6 pages, 2003. View at Publisher · View at Google Scholar · View at Scopus
  20. C. Arpesella, G. Bellini, J. Benziger et al., “First real time detection of 7Be solar neutrinos by Borexino,” Physics Letters B, vol. 658, no. 4, pp. 101–108, 2008. View at Publisher · View at Google Scholar
  21. C. Arpesella, H. O. Back, M. Balata et al., “Direct measurement of the 7Be solar neutrino flux with 192 days of Borexino data,” Physical Review Letters, vol. 101, Article ID 091302, 6 pages, 2008. View at Publisher · View at Google Scholar
  22. R. Becker-Szendy, C. B. Bratton, D. Casper et al., “Electron- and muon-neutrino content of the atmospheric flux,” Physical Review D, vol. 46, no. 9, pp. 3720–3724, 1992. View at Publisher · View at Google Scholar · View at Scopus
  23. D. Casper, R. Becker-Szendy, C. B. Bratton et al., “Measurement of atmospheric neutrino composition with the IMB-3 detector,” Physical Review Letters, vol. 66, no. 20, pp. 2561–2564, 1991. View at Publisher · View at Google Scholar · View at Scopus
  24. K. S. Hirata, K. Inoue, T. Ishida et al., “Observation of a small atmospheric νμ/νe ratio in Kamiokande,” Physics Letters B, vol. 280, no. 1-2, pp. 146–152, 1992. View at Publisher · View at Google Scholar
  25. K. S. Hirata, T. Kajita, M. Koshiba et al., “Experimental study of the atmospheric neutrino flux,” Physics Letters B, vol. 205, no. 2-3, pp. 416–420, 1988. View at Publisher · View at Google Scholar
  26. Y. Fukuda, T. Hayakawa, K. Inoue et al., “Atmospheric νμ/νe ratio in the multi-GeV energy range,” Physics Letters B, vol. 335, pp. 237–245, 1994. View at Google Scholar
  27. M. Aglietta, G. Battistoni, E. Bellotti et al., “Experimental study of atmospheric neutrino flux in the NUSEX experiment,” Europhysics Letters, vol. 8, no. 7, article 611–614, 1989. View at Publisher · View at Google Scholar
  28. Ch. Berger, M. Fröhlich, H. Mönch et al., “Study of atmospheric neutrino interactions with the Fréjus detector,” Physics Letters B, vol. 227, no. 3-4, pp. 489–494, 1989. View at Publisher · View at Google Scholar
  29. K. Daum, W. Rhode, P. Bareyre et al., “Determination of the atmospheric neutrino spectra with the Fréjus detector,” Zeitschrift für Physik C, vol. 66, no. 3, pp. 417–428, 1995. View at Publisher · View at Google Scholar
  30. M. Boliev, A. V. Butkevich, V. N. Zakidyshev et al., “Limitations on parameters of neutrino oscillations according to data of the baksan underground telescope,” Yadernaya Fizika, vol. 34, pp. 1418–1421, 1981, Soviet Journal of Nuclear Physics, vol. 34, pp. 787, 1981. View at Google Scholar
  31. M. M. Boliev, A. V. Butkevich, A. E. Chudakov et al., “Observation of upward through-going muons with the Baksan detector: an update,” Nuclear Physics B, vol. 70, no. 1–3, pp. 371–373, 1999. View at Google Scholar
  32. W. W. M. Allison, G. J. Alner, D. S. Ayres et al., “Measurement of the atmospheric neutrino flavour composition in Soudan 2,” Physics Letters B, vol. 391, pp. 491–500, 1997. View at Publisher · View at Google Scholar
  33. E. Peterson, “Atmospheric neutrino studies in Soudan 2,” Nuclear Physics B, vol. 77, no. 1–3, pp. 111–116, 1999. View at Google Scholar · View at Scopus
  34. M. Ambrosio, R. Antolini, C. Aramo et al., “Measurement of the atmospheric neutrino-induced upgoing muon flux using MACRO,” Physics Letters B, vol. 434, no. 3-4, pp. 451–457, 1998. View at Publisher · View at Google Scholar
  35. F. Ronga, “Atmospheric neutrino induced muons in the MACRO detector,” Nuclear Physics B, vol. 77, no. 1–3, pp. 117–122, 1999. View at Publisher · View at Google Scholar · View at Scopus
  36. P. Bernardini, “Measurement of the Atmospheric Neutrino Induced Muon Flux with the MACRO detector,” in Proceedings of the Vulcano Workshop, Vulcano, Italy, May 1998. View at Publisher · View at Google Scholar
  37. S. P. Ahlen, M. Ambrosio, R. Antolini et al., “Atmospheric neutrino flux measurement using upgoing muons,” Physics Letters B, vol. 357, no. 3, pp. 481–486, 1995. View at Publisher · View at Google Scholar
  38. Y. Fukuda, T. Hayakawa, E. Ichihara et al., “Evidence for oscillation of atmospheric neutrinos,” Physical Review Letters, vol. 81, no. 8, pp. 1562–1567, 1998. View at Publisher · View at Google Scholar
  39. V. Agrawal, T. K. Gaisser, P. Lipari, and T. Stanev, “Atmospheric neutrino flux above 1 GeV,” Physical Review D, vol. 53, no. 3, pp. 1314–1323, 1996. View at Publisher · View at Google Scholar · View at Scopus
  40. M. Honda, T. Kajita, K. Kasahara, and S. Midorikawa, “Calculation of the flux of atmospheric neutrinos,” Physical Review D, vol. 52, no. 9, pp. 4985–5005, 1995. View at Publisher · View at Google Scholar · View at Scopus
  41. M. Honda, T. Kajita, K. Kasahara et al., “Comparison of 3-dimensional and 1-dimensional schemes in the calculation of atmospheric neutrinos,” Physical Review D, vol. 64, Article ID 053011, 12 pages, 2001. View at Publisher · View at Google Scholar
  42. T. Kajita, K. Kasahara, and S. Midorikawa, “New calculation of the atmospheric neutrino flux in a three dimensional scheme,” Physical Review D, vol. 70, no. 4, Article ID 043008, 17 pages, 2004. View at Publisher · View at Google Scholar
  43. G. Battistoni, A. Ferrari, T. Montaruli, and P.R. Sala, “The FLUKA atmospheric neutrino flux calculation,” Astroparticle Physics, vol. 19, no. 2, pp. 269–290, 2003. View at Publisher · View at Google Scholar
  44. G. Altarelli, “Status of the standard model at the LHC start,” Nuovo Cimento della Societa Italiana di Fisica B, vol. 123, no. 3-4, pp. 257–269, 2008. View at Publisher · View at Google Scholar · View at Scopus
  45. G. Giacomelli, “The standard model of particle physics. Neutrino oscillations,” Radiation Measurements, vol. 44, no. 9-10, pp. 826–833, 2009. View at Publisher · View at Google Scholar · View at Scopus
  46. The ALEPH, DELPHI, L3, OPAL, SLD Collab, and The LEP EW Working Group and The SLD EW and Heavy Flavour Groups, “Precision EW measurements on the Z resonance,” Physics Reports, vol. 427, no. 5-6, pp. 257–454, 2006. View at Google Scholar
  47. S. Schael, R. Barate, R. Brunelière et al., “Search for neutral MSSM Higgs bosons at LEP,” The European Physical Journal C, vol. 47, no. 3, pp. 547–587, 2006. View at Publisher · View at Google Scholar
  48. G. Giacomelli and R. Giacomelli, “The LEP legacy,” http://arxiv.org/abs/hep-ex/0503050. View at Publisher · View at Google Scholar
  49. J. Beringer, J.-F. Arguin, R. M. Barnet et al., “Review of particle physics,” Physical Review D, vol. 86, no. 1, Article ID 010001, 1528 pages, 2012. View at Publisher · View at Google Scholar
  50. A. R. Ade, N. Aghanim, and C. Armitage-Caplan, “Planck 2013 results. XVI. Cosmological parameters,” http://arxiv.org/abs/1303.5076.
  51. G. Aad, T. Abajyan, B. Abbott et al., “Observation of a new particle in the search for the SM Higgs boson with the ATLAS detector at the LHC,” Physics Letters B, vol. 716, no. 1, pp. 1–29, 2012. View at Publisher · View at Google Scholar
  52. S. Chatrchyan, V. Khachatryan, A.M. Sirunyan et al., “Observation of a new boson with mass near 125 GeV in pp collisions at sqrt(s) = 7 and 8 TeV,” Physics Letters B, vol. 716, no. 1, pp. 30–61, 2012. View at Publisher · View at Google Scholar
  53. C. Biggio, L. Calibbi, A. Masiero, and S. K. Vempati, “Postcards from oases in the desert: phenomenology of SUSY with intermediate scales,” Journal of High Energy Physics, vol. 1208, article 150, 2012. View at Publisher · View at Google Scholar
  54. T. Schwetz, M. Tórtola, and J. W. F. Valle, “Three-flavour neutrino oscillation update,” New Journal of Physics, vol. 10, Article ID 113011, 2008. View at Publisher · View at Google Scholar · View at Scopus
  55. L. Wolfenstein, “Neutrino oscillations in matter,” Physical Review D, vol. 17, no. 9, pp. 2369–2374, 1978. View at Publisher · View at Google Scholar · View at Scopus
  56. S. P. Mikheyev and A. Yu. Smirnov, “Resonance amplification of oscillations in matter and spectroscopy of solar neutrinos,” Soviet Journal of Nuclear Physics, vol. 42, pp. 913–917, 1985, Il Nuovo Cimento C, vol. 9, pp. 17, 1986. View at Google Scholar
  57. G. Giacomelli and M. Sioli, “Astroparticle physics,” in Lectures at the 6th Constantine School on Weak and Strong Interaction Phenomenology, Constantine, Algeria, 2002.
  58. G. Giacomelli and P. Giacomelli, “Particle searches at LEP,” La Rivista del Nuovo Cimento, vol. 16, no. 3, pp. 1–59, 1993. View at Publisher · View at Google Scholar
  59. R. Barate et al., “An upper limit on the τ neutrino mass from three- and five-prong tau decays,” The European Physical Journal C, vol. 2, no. 3, pp. 395–406, 1998. View at Publisher · View at Google Scholar
  60. C. Arnaboldi, D. R. Artusa, F. T. Avignone et al., “Results from a search for the vββ-decay of 130Te),” Physical Review C, vol. 78, no. 3, Article ID 035502, 5 pages, 2008. View at Publisher · View at Google Scholar
  61. E. Komatsu, K. M. Smith, J. Dunkley et al., “Seven-year wilkinson microwave anisotropy probe (WMAP) observations: cosmological interpretation,” Astrophysical Journal, vol. 192, no. 2, 2011. View at Publisher · View at Google Scholar · View at Scopus
  62. D. W. Sciama, “The present status of the decaying neutrino theory,” Nuclear Physics B, vol. 38, no. 1–3, pp. 320–323, 1995. View at Publisher · View at Google Scholar · View at Scopus
  63. S. Cecchini, D. Centomo, G. Giacomelli et al., “New lower limits on the lifetime of heavy neutrino radiative decay,” Astroparticle Physics, vol. 34, no. 6, pp. 486–492, 2011. View at Publisher · View at Google Scholar · View at Scopus
  64. F. Reines, M. F. Crouch, T. L. Jenkins et al., “Evidence for high-energy cosmic-ray neutrino interactions,” Physical Review Letters, vol. 15, no. 9, pp. 429–433, 1965. View at Publisher · View at Google Scholar · View at Scopus
  65. C. V. Achar, M. G. K. Menon, V. S. Narasimham et al., “Detection of muons produced by cosmic ray neutrinos deep underground,” Physics Letters, vol. 18, no. 2, pp. 196–199, 1965. View at Publisher · View at Google Scholar · View at Scopus
  66. Y. Ashie, J. Hosaka, K. Ishihara et al., “Evidence for an oscillatory signature in atmospheric neutrino oscillations,” Physical Review Letters, vol. 93, no. 10, Article ID 101801, 2004. View at Publisher · View at Google Scholar · View at Scopus
  67. Y. Ashie, J. Hosaka, K. Ishihara et al., “Measurement of atmospheric neutrino oscillation parameters by Super-Kamiokande I,” Physical Review D, vol. 71, no. 11, Article ID 112005, 35 pages, 2005. View at Publisher · View at Google Scholar
  68. M. Ambrosio, R. Antolini, D. Bakari et al., “Measurements of atmospheric muon neutrino oscillations, global analysis of the data collected with MACRO detector,” The European Physical Journal C, vol. 36, no. 3, pp. 323–339, 2004. View at Publisher · View at Google Scholar
  69. W. W. M. Allison, G. J. Alner, D. S. Ayres et al., “The atmospheric neutrino flavor ratio from a 3.9 fiducial kiloton-year exposure of Soudan 2,” Physics Letters B, vol. 449, no. 1-2, pp. 137–144, 1999. View at Publisher · View at Google Scholar · View at Scopus
  70. M. Sanchez, W. W. M. Allison, G. J. Alner et al., “Measurement of the L/E distributions of atmospheric v in Soudan 2 and their interpretation as neutrino oscillations,” Physical Review D, vol. 68, no. 11, Article ID 113004, 14 pages, 2003. View at Publisher · View at Google Scholar
  71. M. Ambrosio, R. Antolini, R. Assiro et al., “The MACRO detector at Gran Sasso,” Nuclear Instruments and Methods in Physics Research A, vol. 486, no. 3, pp. 663–707, 2002. View at Publisher · View at Google Scholar
  72. M. Ambrosio, R. Antolini, D. Bakari et al., “Atmospheric neutrino oscillations from upward throughgoing muon multiple scattering in MACRO,” Physics Letters B, vol. 566, no. 1-2, pp. 35–44, 2003. View at Publisher · View at Google Scholar · View at Scopus
  73. M. Ambrosio, R. Antolini, G. Auriemma et al., “Low energy atmospheric muon neutrinos in MACRO,” Physics Letters B, vol. 478, no. 1–3, pp. 5–13, 2000. View at Publisher · View at Google Scholar
  74. M. Ambrosio, R. Antolini, G. Auriemma et al., “Matter effects in upward-going muons and sterile neutrino oscillations,” Physics Letters B, vol. 517, no. 1-2, pp. 59–66, 2001. View at Publisher · View at Google Scholar
  75. Y. Fukuda, S. Fukuda, M. Ishitsuka et al., “Tau neutrinos favored over sterile neutrinos in atmospheric muon neutrino oscillations,” Physical Review Letters, vol. 85, no. 19, pp. 3999–4003, 2000. View at Publisher · View at Google Scholar · View at Scopus
  76. G. Giacomelli and M. Giorgini, “Atmospheric neutrino oscillations,” in Lecture at the 7th School on Non-Accelerator Astroparticle Physics, Trieste, Italy, 2004.
  77. Y. Fukuda, T. Hayakawa, E. Ichihara et al., “Measurement of the flux and zenith angle distribution of upward through-going muons by Super Kamiokande,” Physical Review Letters, vol. 82, no. 13, pp. 2644–2648, 1999. View at Publisher · View at Google Scholar
  78. R. Wendell, C. Ishihara, K. Abe et al., “Atmospheric neutrino oscillation analysis with subleading effects in Super-Kamiokande I, II and III,” Physical Review D, vol. 81, Article ID 092004, 16 pages, 2010. View at Publisher · View at Google Scholar
  79. G. L. Fogli, E. Lisi, A. Marrone, and G. Scioscia, “Testing violations of special and general relativity through the energy dependence of νμντ oscillations in the Super-Kamiokande atmospheric neutrino experiment,” Physical Review D, vol. 60, no. 5, pp. 1–9, 1999. View at Google Scholar · View at Scopus
  80. G. L. Fogli, E. Lisi, A. Marrone, and G. Scioscia, “Super-Kamiokande data and atmospheric neutrino decay,” Physical Review D, vol. 59, no. 11, Article ID 117303, 3 pages, 1999. View at Publisher · View at Google Scholar
  81. Y. Suzuki, “Super-Kamiokande,” in Proceedings of the 16th Workshop on Neutrino Telescopes, Venezia, Italy, 2013.
  82. K. Abe, Y. Hayato, T. Iida et al., “A measurement of the appearance of atmospheric tau neutrinos by SuperK,” Physical Review Letters, vol. 110, no. 18, Article ID 181802, 7 pages, 2013. View at Publisher · View at Google Scholar
  83. T. Kajita, “Discovery of neutrino oscillations,” Reports on Progress in Physics, vol. 69, no. 6, pp. 1607–1635, 2006. View at Publisher · View at Google Scholar · View at Scopus
  84. G. Giacomelli, “Atmospheric ν's and long baseline neutrino experiments,” in AIP Conference Proceedings, vol. 972, pp. 412–420, Sinaia, Romania, 2008. View at Publisher · View at Google Scholar
  85. G. C. Trinchero, M. Ambrosio, M. Amelchakov et al., “MONOLITH: a massive magnetized iron detector for atmospheric neutrinos,” in Proceedings of the 27th International Cosmic Ray Conference, Hamburg, Germany, August 2001.
  86. N. K. Mondal, “India-based Neutrino Observatory,” Pramana, vol. 79, p. 1003, 2012. View at Publisher · View at Google Scholar
  87. M. Apollonio, A. Baldini, C. Bemporad et al., “Search for neutrino oscillations on a long base-line at the chooz nuclear power station,” European Physical Journal C, vol. 27, no. 3, pp. 331–374, 2003. View at Publisher · View at Google Scholar · View at Scopus
  88. F. Boehm, J. Busenitz, B. Cook et al., “Final results from the Palo Verde neutrino oscillation experiment,” Physical Review D, vol. 64, no. 11, Article ID 112001, 2001. View at Google Scholar · View at Scopus
  89. F. P. An, J. Z. Bai1, A. B. Balantekin et al., “Observation of electron-antineutrino disappearance at Daya Bay,” Physical Review Letters, vol. 108, no. 17, Article ID 171803, 7 pages, 2012. View at Publisher · View at Google Scholar
  90. F. P. An, Q. An, J. Z. Bai et al., “Improved measurement of electron antineutrino disappearance at Daya Bay,” Chinese Physics C, vol. 37, no. 1, Article ID 011001, 2013. View at Publisher · View at Google Scholar
  91. J. Cao, “Daya Bay: results and future,” in Proceedings of the 16th Workshop on Neutrino Telescopes, Venezia, Italy, 2013.
  92. Y. Abe, “First measurement of θ13 from delayed neutron capture on hydrogen in the Double Chooz experiment,” Physics Letters B, vol. 723, no. 1–3, pp. 66–70, 2013. View at Publisher · View at Google Scholar
  93. A. Cabrera, “Double chooz,” in Proceedings of the 16th Workshop on Neutrino Telescopes, Venezia, Italy, 2013. View at Publisher · View at Google Scholar
  94. S.-H. Seo, “New results from RENO,” in Proceedings of the 16th Workshop on Neutrino Telescopes, Venezia, Italy, 2013. View at Publisher · View at Google Scholar
  95. J. K. Ahn, S. Chebotaryov, J. H. Choi et al., “Observation of reactor electron antineutrino disappearance in the RENO experiment,” Physical Review Letters, vol. 108, no. 19, Article ID 191802, 6 pages, 2012. View at Publisher · View at Google Scholar
  96. T2K exp, “T2K Observes νμ>νe  definitively,” CERN Courier, vol. 2013, 8 pages.
  97. S. Pascoli, “A theoretical perspective on neutrinos,” in Proceedings of the 26th International Lepton Photon Symposium, San Francisco, Calif, USA, 2013.
  98. S. Dusini, A. Longhin, M. Mezzetto et al., “CP violation and mass hierarchy at medium baselines in the large teta13 era,” Europhysics Journal, vol. C73, p. 2392, 2013. View at Google Scholar
  99. M. Gribier, “Reactor antineutrino anomalies and searches for sterile neutrinos in Europe,” in Proceedings of the 16th Workshop on Neutrino Telescopes, Venezia, Italy, 2013.
  100. P. K. Huber, “Reactor neutrinos-fluxes and US Plans,” in Proceedings of the 16th Workshop on Neutrino Telescopes, Venezia, Italy, 2013.
  101. J. Kopp, “Global status of sterile neutrino scenario,” in Proceedings of the 16th Workshop on Neutrino Telescopes, Venezia, 2013.
  102. M. H. Ahn, E. Aliu, S. Andringa et al., “Measurement of neutrino oscillation by the K2K experiment,” Physical Review D, vol. 74, no. 7, Article ID 072003, 39 pages, 2006. View at Publisher · View at Google Scholar
  103. E. Aliu, S. Andringa, S. Aoki et al., “Evidence for muon neutrino oscillations in an accelerator-based experiment,” Physical Review Letters, vol. 94, no. 8, Article ID 081802, 5 pages, 2005. View at Publisher · View at Google Scholar
  104. P. Adamson, I. Anghel, C. Backhouse et al., “Measurement of neutrino and antineutrino oscillations using beam and atmospheric data in MINOS,” Physical Review Letters, vol. 110, no. 25, Article ID 251801, 6 pages, 2013. View at Publisher · View at Google Scholar
  105. K. Lang, “MINOS selected topics,” in Proceedings of the 16th Workshop on Neutrino Telescopes, Venezia, Italy, 2013.
  106. V. Barger, J. G. Learned, P. Lipari, M. Lusignoli, S. Pakvasa, and T. J. Weiler, “Neutrino decay and atmospheric neutrinos,” Physics Letters B, vol. 462, no. 1-2, pp. 109–114, 1999. View at Publisher · View at Google Scholar · View at Scopus
  107. E. Lisi, A. Marrone, and D. Montanino, “Probing possible decoherence effects in atmospheric neutrino oscillations,” Physical Review Letters, vol. 85, no. 6, pp. 1166–1169, 2000. View at Publisher · View at Google Scholar · View at Scopus
  108. P. Adamson, C. Andreopoulos, K. E. Arms et al., “Meaurement of neutrino oscillations with the MINOS detectors in the NuMi beam,” Physical Review Letters, vol. 101, no. 13, Article ID 131802, 2008. View at Google Scholar
  109. P. Adamson, C. Andreopoulos, K. E. Arms et al., “Study of muon neutrino disappearance using the Fermilab Main Injector neutrino beam,” Physical Review D, vol. 77, no. 1, Article ID 072002, 2008. View at Publisher · View at Google Scholar
  110. E. Eskut, A. Kayis-Topaksu, G. Önengüt et al., “Final results on νμντ oscillations from the CHORUS experiment,” Nuclear Physics B, vol. 793, no. 1-2, pp. 326–343, 2008. View at Publisher · View at Google Scholar
  111. P. Astier, D. Autiero, A. Baldisseri et al., “Final NOMAD results on νμνe and νeντ oscillations including a new search for ντ appearance using hadronic tau decays,” Nuclear Physics B, vol. 611, no. 1–3, pp. 3–39, 2001. View at Publisher · View at Google Scholar
  112. R. Acquafredda, T. Adam, N. Agafonova et al., “The OPERA experiment in the CERN to Gran Sasso neutrino beam,” Journal of Instrumentation, vol. 4, Article ID P04018, 2009. View at Google Scholar
  113. R. Acquafredda, N. Agafonova, M. Ambrosio et al., “First events from the CNGS neutrino beam detected in the OPERA experiment,” New Journal of Physics, vol. 8, article 303, 2006. View at Google Scholar
  114. N. Agafonova, A. Anokhina, S. Aoki et al., “The detection of neutrino interactions in the emulsion/lead target of the OPERA experiment,” Journal of Instrumentation, vol. 4, Article ID P06020, 2009. View at Publisher · View at Google Scholar
  115. A. Anokhina, S. Aoki, A. Ariga et al., “Emulsion sheet doublets as interface trackers for the OPERA experiment,” Journal of Instrumentation, vol. 3, Article ID P07005, 2008. View at Publisher · View at Google Scholar
  116. L. Arrabito, E. Barbuto, C. Bozza et al., “Hardware performance of a scanning system for high speed analysis of nuclear emulsions,” Nuclear Instruments and Methods in Physics Research A, vol. 568, no. 2, pp. 578–587, 2006. View at Publisher · View at Google Scholar
  117. L. Arrabito, D. Autiero, C. Bozza et al., “Electron/pion separation with an Emulsion Cloud Chamber by using a Neural Network,” Journal of Instrumentation, vol. 2, Article ID P02001, 2007. View at Publisher · View at Google Scholar
  118. M. De Serio, M. Ieva, S. Simone et al., “Momentum measurement by the angular method in the Emulsion Cloud Chamber,” Nuclear Instruments and Methods in Physics Research A, vol. 512, no. 3, pp. 539–545, 2003. View at Publisher · View at Google Scholar
  119. N. Armenise, M. De Serio, M. Ieva et al., “High-speed particle tracking in nuclear emulsion by last-generation automatic microscopes,” Nuclear Instruments and Methods in Physics Research A, vol. 551, no. 2-3, pp. 261–270, 2005. View at Google Scholar
  120. S. Balestra, A. Bertolini, C. Bozza et al., “A fast automatic plate changer for the analysis of nuclear emulsions,” Nuclear Instruments and Methods in Physics Research A, vol. 716, pp. 96–100, 2013. View at Publisher · View at Google Scholar
  121. T. Fukuda, K. Kodamab, M. Komatsu et al., “The analysis of interface emulsion detector for the OPERA experiment in JAPAN Scanning facility,” Journal of Instrumentation, vol. 5, Article ID P04009, 2010. View at Publisher · View at Google Scholar
  122. N. Agafonova, A. Aleksandrov, O. Altino et al., “Observation of a first ντ candidate event in the OPERA experiment in the CNGS beam,” Physics Letters B, vol. 691, no. 3, pp. 138–145, 2010. View at Publisher · View at Google Scholar
  123. G. De Lellis, “New results from the OPERA experiment,” CERN Seminar, 2013.
  124. N. Agafonova, A. Aleksandrov, A. Anokhina et al., “New Results on νμντ appearance with the OPERA experiment in the CNGS beam,” 2013, http://arxiv.org/abs/1308.2553.
  125. N. Agafonova, A. Aleksandrov, A. Anokhina et al., “Search for νμνe oscillations with the OPERA experiment in the CNGS beam,” Journal of High Energy Physics, vol. 07, article 004, 2013. View at Google Scholar
  126. T. Adam, N. Agafonova, A. Aleksandrov et al., “Measurement of the neutrino velocity with the OPERA detector in the CNGS beam,” Journal of High Energy Physics, vol. 10, article 093, 2012. View at Google Scholar
  127. T. Adam, N. Agafonova, A. Aleksandrov et al., “Measurement of the neutrino velocity with the OPERA detector in the CNGS beam using the 2012 dedicated data,” Journal of High Energy Physics, vol. 01, article 153, 2013. View at Google Scholar
  128. S. Bertolucci, “Neutrino speed: a report on the νμ speed measurements of the BOREXINO, ICARUS and LVD experiments with the CNGS beam,” Nuclear Physics B, vol. 235-236, pp. 289–295, 2013. View at Publisher · View at Google Scholar
  129. M. Antonello, B. Baibussinov, P. Benetti et al., “Experimental search for the LSND anomaly with the ICARUS detector in the CNGS neutrino beam,” The European Physical Journal C, vol. C73, p. 2345, 2013. View at Google Scholar
  130. F. Pietropaolo, “Status of the ICARUS experiment,” Nuclear Physics B, vol. 235-236, pp. 115–121, 2013. View at Google Scholar
  131. T. Nakaya, “Results and prospects of the T2K neutrino experiment,” Conference: C11-10-24.1, Proceedings, p. 64, http://www.worldscientific.com/doi/abs/10.1142/9789814412322 0007.
  132. K. Abe, N. Abgrall, H. Aihara et al., “Evidence of electron neutrino appearance in a muon neutrino beam,” Physical Review D, vol. 88, no. 3, 41 pages, 2013. View at Publisher · View at Google Scholar
  133. K. Abeaw, N. Abgrall, H. Aihara et al., “The T2K experiment,” Nuclear Instruments and Methods in Physics Research Section A, vol. 659, no. 1, pp. 106–135, 2011. View at Publisher · View at Google Scholar
  134. K. Abe, N. Abgrall, Y. Ajima et al., “First muon-neutrino disappearance study with an off-axis beam,” Physical Review D, vol. 85, Article ID 031103, 8 pages, 2012. View at Publisher · View at Google Scholar
  135. T. Kobayashi, “T2K experiment,” in Proceedings of the 16th Workshop on Neutrino Telescopes, Venezia, Italy, 2013.
  136. L. A. Corwin, “(Status of NOνA),” in Proceedings of the 16th Workshop on Neutrino Telescopes, Venezia, Italy, 2013.
  137. C. Athanassopoulos, L. B. Auerbach, R. L. Burman et al., “Results on νμνe neutrino oscillations from the LSND experiment,” Physical Review Letters, vol. 81, no. 9, pp. 1774–1777, 1998. View at Publisher · View at Google Scholar
  138. A. Aguilar, L. B. Auerbach, R. L. Burman et al., “Evidence for neutrino oscillations from the observation of v¯e appearance in a v¯μ beam),” Physical Review D, vol. 64, no. 11, Article ID 112007, 22 pages, 2001. View at Publisher · View at Google Scholar
  139. B. Armbruster, I. M. Blair, B. A. Bodmann et al., “Upper limits for neutrino oscillations v¯μv¯e from muon decay at rest,” Physical Review D, vol. 65, no. 11, Article ID 112001, 16 pages, 2002. View at Publisher · View at Google Scholar
  140. A. A. Aguilar-Arevalo, C. E. Anderson, S. J. Brice et al., “Event Excess in the MiniBooNE Search for v¯μv¯e oscillations,” Physical Review Letters, vol. 105, no. 18, Article ID 181801, 5 pages, 2010. View at Publisher · View at Google Scholar
  141. X.-Q. Li, Y. Liu, Z.-T. Wei, and L. Tang, “Neutrino decay as a possible interpretation of the MiniBooNE observation with unparticle scenario,” European Physical Journal C, vol. 56, no. 1, pp. 97–103, 2008. View at Publisher · View at Google Scholar · View at Scopus
  142. M. Maltoni and T. Schwetz, “Sterile neutrino oscillations after first MiniBooNE results,” Physical Review D, vol. 76, no. 9, Article ID 093005, 2007. View at Publisher · View at Google Scholar · View at Scopus
  143. G. Mention, M. Fechner, Th. Lasserre et al., “The Reactor Antineutrino Anomaly,” Physical Review D, vol. 83, no. 7, Article ID 073006, 20 pages, 2011. View at Publisher · View at Google Scholar
  144. C. Giunti and M. Laveder, “Statistical significance of the gallium anomaly,” Physical Review C, vol. 83, no. 6, Article ID 065504, 2011. View at Publisher · View at Google Scholar · View at Scopus
  145. A. C. Hayes, J. L. Friar, G. T. Garvey, and G. Jonkmans, “Reanalysis of the reactor neutrino anomaly,” http://arxiv.org/abs/1309.4146.
  146. C. Giunti, M. Laveder, Y. F. Li, and H. W. Long, “A Pragmatic view of short-baseline neutrino oscillations,” Physical Review D, vol. 88, no. 7, 6 pages, 2013. View at Publisher · View at Google Scholar
  147. S. Razzaque and A. Y. Smirnov, “Searching for sterile neutrinos in ice,” Journal of High Energy Physics, vol. 1107, article 084, 2011. View at Google Scholar
  148. G. Bellini, J. Benziger, D. Bick et al., “SOX: short distance neutrino Oscillations with BoreXino,” Journal of High Energy Physics, vol. 1308, article 038, 2013. View at Google Scholar
  149. P. Bernardini, A. Bertolin, C. Bozza et al., “Prospect for charge current neutrino interactions measurements at the CERN-PS,” http://arxiv.org/abs/1111.2242.
  150. M. Antonello, D. Bagliani, B. Baibussinov et al., “Search for anomalies in the neutrino sector with muon spectrometers and large LArTPC imaging detectors at CERN,” http://arxiv.org/abs/1208.0862.
  151. M. Antonello, D. Bagliani, B. Baibussinov et al., “Search for anomalies from neutrino and anti-neutrino oscillations at Δm2~1eV2 with muon spectrometers and large LArTPC imaging detectors,” http://arxiv.org/abs/1203.3432.
  152. A. B. Sousa, “MINOS search for sterile neutrinos,” Journal of Physics: Conference Series, vol. 408, no. 1, Article ID 012026, 2013. View at Publisher · View at Google Scholar
  153. M. C. Gonzalez-Garcia and M. Maltoni, “Atmospheric neutrino oscillations and new physics,” Physical Review D, vol. 70, no. 3, Article ID 033010, 2004. View at Publisher · View at Google Scholar · View at Scopus
  154. G. Battistoni, Y. Becherini, S. Cecchini et al., “Search for a Lorentz invariance violation contribution in atmospheric neutrino oscillations using MACRO data,” Physics Letters B, vol. 615, no. 1-2, pp. 14–18, 2005. View at Publisher · View at Google Scholar · View at Scopus
  155. P. Adamson, C. Andreopoulos, K. E. Arms et al., “Testing Lorentz invariance and CPT conservation with NuMI neutrinos in the MINOS near detector,” Physical Review Letters, vol. 101, no. 15, Article ID 151601, 2008. View at Google Scholar
  156. P. A. N. MacHado, H. Nunokawa, and R. Z. Funchal, “Testing for large extra dimensions with neutrino oscillations,” Physical Review D, vol. 84, no. 1, Article ID 013003, 2011. View at Publisher · View at Google Scholar · View at Scopus
  157. J. Adam, X. Bai, A. M. Baldini et al., “New constraint on the existence of the mu+->e+ gamma decay,” Physics Review Letters, vol. 110, Article ID 201801, 5 pages, 2013. View at Publisher · View at Google Scholar
  158. M. G. Catanesi, E. Radicioni, R. Edgecock et al., “Large-angle production of charged pions by 3-12.9GeV/c protons on beryllium, aluminium and lead targets,” European Physical Journal C, vol. 54, no. 1, pp. 37–60, 2008. View at Publisher · View at Google Scholar · View at Scopus
  159. K. Hiraide, J. L. Alcaraz-Aunion, S. J. Brice et al., “Search for charged current coherent pion production on carbon in a few-GeV neutrino beam,” Physical Review D, vol. 78, no. 11, Article ID 112004, 19 pages, 2008. View at Publisher · View at Google Scholar
  160. Y. Kurimoto, J. L. Alcaraz-Aunion, S. J. Brice et al., “Measurement of inclusive neutral current Pion production on carbon in a few-GeV neutrino beam,” Physical Review D, vol. 81, Article ID 033004, 2010. View at Publisher · View at Google Scholar
  161. A. Laszlo, “The NA61/SHINE experiment at the CERN SPS,” Nuclear Physics A, vol. 830, no. 1–4, pp. 559c–562c, 2009. View at Publisher · View at Google Scholar
  162. M. Gazdzicki, Z. Fodor, and G. Vesztergombi, “Study of hHadron production in hadron-nucleus and nucleus-nucleus collisions at the CERN SPS,” SPSC-P-330; CERN-SPSC-2006-034, http://cdsweb.cern.ch/record/995681/files/.
  163. B. A. Popov, “Hadron production experiments and their implications on neutrino physics,” in International Conference on Neutrino Physics and Astrophysics, Kyoto, Japan, 2012.
  164. T. Kafka and V. Paolone, “Prospects and status of the MINERνA experiment at FNAL,” Progress in Particle and Nuclear Physics, vol. 64, no. 2, pp. 181–183, 2010. View at Publisher · View at Google Scholar · View at Scopus
  165. V. Paolone, “MINERvA: status and prospect,” in Proceedings of the 16th Workshop on Neutrino Telescopes, Venezia, Italy, 2013. View at Publisher · View at Google Scholar
  166. J. Spitz, “ArgoNeuT, a liquid argon time projection chamber in a low energy neutrino beam,” Journal of Physics: Conference Series, vol. 203, Article ID 012108, 2010. View at Publisher · View at Google Scholar · View at Scopus
  167. F. Cavanna, “The ArgoNeuT LAr TPC: a dedicated experiment for cross section measurements at FNAL,” in Proceedings of the 23rd International Workshop on Weak Interactions and Neutrinos (WIN ’11), Cape Town, South Africa, January 2011.
  168. T. Chiarusi and M. Spurio, “High-energy astrophysics with neutrino telescopes,” European Physical Journal C, vol. 65, no. 3, pp. 649–701, 2009. View at Publisher · View at Google Scholar · View at Scopus
  169. A. Avrorin et al., “The Baikal neutrino experiment: results and plans,” Nuclear Instruments and Methods in Physics A, vol. 630, pp. 115–118, 2011. View at Publisher · View at Google Scholar
  170. M. Ackermann, J. Adams, J. Ahrens et al., “Search for ultra-high-energy Neutrinos with AMANDA-II,” The Astrophysical Journal, vol. 675, no. 2, p. 1014, 2008. View at Publisher · View at Google Scholar
  171. R. Abbasi, Y. Abdou, T. Abu-Zayyad et al., “Limits on a muon flux from Kaluza-Klein dark matter annihilations in the Sun from the IceCube 22-string detector,” Physical Review D, vol. 81, no. 5, Article ID 057101, 6 pages, 2010. View at Publisher · View at Google Scholar
  172. E. Resconi, “Neutrino telescope: IceCube,” in Proceedings of the Neutrino, Athens, Ga, USA, 2010.
  173. S. Odrowski, “Recent results from the IceCube neutrino telescope,” Acta Physica Polonica B, vol. 6, no. 2, p. 687, 2013. View at Google Scholar
  174. P. Amram, M. Anghinolfi, S. Anvar et al., “The ANTARES optical module,” Nuclear Instruments and Methods in Physics Research A, vol. 484, no. 1–3, pp. 369–383, 2002. View at Publisher · View at Google Scholar
  175. S. Adrian-Martinez, I. Al Samarai, A. Albert et al., “Search for cosmic neutrino point sources with four year data of the ANTARES telescope,” The Astrophysical Journal, vol. 760, no. 1, p. 53, 2012. View at Publisher · View at Google Scholar
  176. S. Adrián-Martínez, I. Al Samarai, A. Albertc et al., “Measurement of atmospheric neutrino oscillations with the ANTARES neutrino telescope,” Physics Letters B, vol. 714, no. 2–5, pp. 224–230, 2012. View at Publisher · View at Google Scholar
  177. P. Sapienza, “KM3NeT, Multi-Km3 neutrino telescope: perspectives,” in Proceedings of the 16th Workshop on Neutrino Telescopes, Venezia, Italy, 2013. View at Publisher · View at Google Scholar
  178. R. Abbasi, Y. Abdou, T. Abu-Zayyad et al., “A Search for a diffuse flux of astrophysical muon neutrinos with the IceCube 40-string detector,” Physical Review D, vol. 84, no. 8, Article ID 082001, 20 pages, 2011. View at Publisher · View at Google Scholar
  179. M. G. Aartsen, R. Abbasi, Y. Abdou et al., “Measurement of atmospheric neutrino oscillations with Ice-Cube,” Physical Review Letters, vol. 111, no. 8, Article ID 081801, 6 pages, 2013. View at Publisher · View at Google Scholar
  180. R. Abbasi, Y. Abdou, T. Abu-Zayyad et al., “Search for a Lorentz-violating sidereal signal with atmospheric neutrinos in IceCube,” Physical Review D, vol. 82, no. 11, Article ID 112003, 6 pages, 2010. View at Publisher · View at Google Scholar
  181. M. G. Aarsten, R. Abbasi, Y. Abdou et al., “Measurement of the atmospheric ve flux in IceCube,” Physical Review Letters, vol. 110, no. 15, Article ID 151105, 7 pages, 2013. View at Publisher · View at Google Scholar
  182. L. A. Fusco, “Measurement of the atmospheric νμ energy spectrum with the ANTARES neutrino telescope,” in ICRC Conference, 2013. View at Publisher · View at Google Scholar
  183. L. A. Fusco and V. Kalinowsky, “Measurement of the atmospheric νμ energy spectrum with the ANTARES neutrino telescope,” in ICRC Conference, 2013. View at Publisher · View at Google Scholar
  184. S. Biagi, “Updated limits on diffuse fluxes of cosmic neutrinos with 2008–2011 ANTARES data,” http://arxiv.org/abs/1305.6442. View at Publisher · View at Google Scholar
  185. V. Barger, D. Marfatia, and K. Whisnant, “Breaking eightfold degeneracies in neutrino CP violation, mixing, and mass hierarchy,” Physical Review D, vol. 65, no. 7, Article ID 073023, pp. 730231–7302317, 2002. View at Google Scholar · View at Scopus
  186. G. L. Fogli, E. Lisi, A. Marrone et al., “A global analysis of neutrino oscillations,” Nuclear Physics B, vol. 235-236, pp. 125–132, 2013. View at Publisher · View at Google Scholar
  187. R. Battistoni, M. Mezzetto, P. Migliozzi, and F. Terranova, “European facilities for accelerator neutrino physics: perspectives for the decade to come,” Rivista del Nuovo Cimento, vol. 33, no. 6, pp. 313–343, 2010. View at Publisher · View at Google Scholar · View at Scopus
  188. T. Nakaya, “Hyper-kamiokande,” in Proceedings of the 16th Workshop on Neutrino Telescopes, Venezia, Italy, 2013.
  189. C. Walter, “Atmospheric neutrinos: overview and opportunities,” in Proceedings of the 16th Workshop on Neutrino Telescopes, Venezia, Italy, 2013.
  190. R. N. Mohapatra, “Neutrinos and the LHC,” in Proceedings of the Neutrino, Athens, Ga, USA, 2010. View at Publisher · View at Google Scholar